zeolite
Brilliant_Rock
- Joined
- Aug 13, 2008
- Messages
- 619
Gems & Gemology is a leading journal of accurate scientific information on gemstones. The three most important issues in the 30+ year history of this journal were “an update to color in gems”:
Volume XXIII, Fall 1987, pages 126-139, “Introduction and colors caused by dispersed metal ions”
Volume XXIV, Spring 1988, pages 3-15, “Colors involving multiple atoms and color centers”
Volume XXIV, Summer 1988, pages 81-102, “Colors caused by band gaps and physical phenomena”
Since my collection of Gems & Gemology is second only to GIA, I will quote sections of these difficult to find, older issues.
This post is in response to another thread on alexandrite w/vanadium. I will not take sides or discuss fluorescence. I will just quote sections concerning alexandrite, chromium, vanadium, and other color change stones.
Fall 1987, page 138, table 1 (dispersed metal ions and the colors they cause in various gem materials)
V3+ octahedral color-change effect: corundum and some rare pyropes and pyrope-spessartine
(my comment: V3+ means tri-valent vanadium in octahedral crystal coordination)
Cr3+ octahedral color-change effect: chrysoberyl/alexandrite: some pyropes
(my comment: Cr3+ means tri-valent chromium in octahedral crystal coordination)
Spring 1988 page 31 Chrysoberyl and Alexandrite from the Pegmatite Districts of Minas Gerais, Brazil
The Hematita alexandrites contain 0.30-0.44 wt % Cr2O3, 1.11-1.59 wt % Fe2O3, and 0.01-0.03 wt % V2O3
Summer 1988, page 95, table 4 (causes of color on most gem materials)
Color change (alexandrite) Cr3+ in octahedral coordination
Color change (corundum) Cr3+ and/or V3+ in octrahedral coordination in a particular range of concentration
Volume XXIII, Fall 1987, pages 126-139, “Introduction and colors caused by dispersed metal ions”
Volume XXIV, Spring 1988, pages 3-15, “Colors involving multiple atoms and color centers”
Volume XXIV, Summer 1988, pages 81-102, “Colors caused by band gaps and physical phenomena”
Since my collection of Gems & Gemology is second only to GIA, I will quote sections of these difficult to find, older issues.
This post is in response to another thread on alexandrite w/vanadium. I will not take sides or discuss fluorescence. I will just quote sections concerning alexandrite, chromium, vanadium, and other color change stones.
Fall 1987, page 138, table 1 (dispersed metal ions and the colors they cause in various gem materials)
V3+ octahedral color-change effect: corundum and some rare pyropes and pyrope-spessartine
(my comment: V3+ means tri-valent vanadium in octahedral crystal coordination)
Cr3+ octahedral color-change effect: chrysoberyl/alexandrite: some pyropes
(my comment: Cr3+ means tri-valent chromium in octahedral crystal coordination)
Spring 1988 page 31 Chrysoberyl and Alexandrite from the Pegmatite Districts of Minas Gerais, Brazil
The Hematita alexandrites contain 0.30-0.44 wt % Cr2O3, 1.11-1.59 wt % Fe2O3, and 0.01-0.03 wt % V2O3
Summer 1988, page 95, table 4 (causes of color on most gem materials)
Color change (alexandrite) Cr3+ in octahedral coordination
Color change (corundum) Cr3+ and/or V3+ in octrahedral coordination in a particular range of concentration